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Algorithm development for snow destiny estimation using polarimetric advanced SAR Data

机译:利用极化高级SAR数据进行雪况估计的算法开发

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Remote sensing of Radar Polarimety has great potential to determine the extent and properties of snow cover. Availability of spaceborne sensor dual polarimetric C-band data of ENVISAT-ASAR can enhance the accuracy in measurement of snow physical parameters as compared to single fixed polarization data measurement. This study shows that the capability of C-band SAR data for estimating dry snow density over snow coverer rugged terrain in Himalayan region. The study area lies in Beas, Chandra and Bhaga catchments of Himachal state (India). For this investigation, the main assumptions are that the snow is dry and at C-band, total backscattering coefficient comes from snowpack and snow ground interface. An algorithm for estimating snow density has been developed based on snow volume scattering and snow-ground scattering components. Snow density estimation algorithm requires HH and VV polarization combination data. The radar backscattering coefficients of both HH and VV polarization and incidence angle are given as input to the developed algorithm. Finally, the algorithm gives the snow dielectric constant which can further be related to snow density using Looyenga's semi empirical formula. Comparison was done between algorithm estimated snow density and field value of snow density in the study region. The mean absolute error between estimated and measured snow density was 21.3 kg/m~3.
机译:雷达极化的遥感具有确定积雪范围和性质的巨大潜力。与单固定极化数据测量相比,ENVISAT-ASAR的星载传感器双极化C波段数据的可用性可以提高雪物理参数的测量精度。这项研究表明,C波段SAR数据能够估算喜马拉雅地区积雪覆盖崎terrain地形上的干雪密度。研究区域位于喜马al尔州(印度)的比斯,钱德拉和巴加流域。对于此调查,主要假设是雪是干燥的,在C波段,总的反向散射系数来自积雪和雪地界面。已经基于雪量散射和雪地散射分量开发了一种估计雪密度的算法。雪密度估算算法需要HH和VV极化组合数据。给出了HH和VV极化以及入射角的雷达后向散射系数作为所开发算法的输入。最后,该算法使用Looyenga的半经验公式给出了雪的介电常数,该常数可以进一步与雪的密度相关。算法估计的雪密度与研究区域的雪密度场值之间进行了比较。估计和测得的雪密度之间的平均绝对误差为21.3 kg / m〜3。

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